Cooperative Geological Geophysical Geochemical Investigation Of Geothermal Resources In The Imperial Valley Area Of California
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Journal of Research
Author | : Geological Survey (U.S.) |
Publisher | : |
Total Pages | : 892 |
Release | : 1977 |
Genre | : Cartography |
ISBN | : |
Journal of Research of the U.S. Geological Survey
Author | : Geological Survey (U.S.) |
Publisher | : |
Total Pages | : 472 |
Release | : 1977 |
Genre | : Geology |
ISBN | : |
Scientific notes and summaries of investigations in geology, hydrology, and related fields.
Geothermal Resource and Reservoir Investigations of U.S. Bureau of Reclamation Leaseholds at East Mesa, Imperial Valley, California
Author | : Lawrence Berkeley Laboratory. Earth Sciences Division |
Publisher | : |
Total Pages | : 326 |
Release | : 1978 |
Genre | : Geothermal resources |
ISBN | : |
Geothermal Energy; East Mesa Geothermal Field; Geochemical Surveys; Geology; Geothermal Fluids; Geothermal Wells; Seismicity; Simulation; Chemical Composition; Scaling; Flow Rate; Salton Sea; Brines; Ammonia; Carbon Dioxide; Ground Subsidence; Performance Testing; Reinjection; Reservoir Pressure; Reservoir Temperature; Salton Sea Geothermal Field; Transients; California; Carbon Compounds; Carbon Oxides; Chalcogenides; Fluids; Geothermal Fields; Hydrides; Hydrogen Compounds; Imperial Valley; Nitrogen Compounds; Nitrogen Hydrides; North America; Oxides; Oxygen Compounds; Testing; USA; Wells; Western Region.
Geothermal Resources Exploration & Exploitation
Author | : United States. Energy Research and Development Administration. Technical Information Center |
Publisher | : |
Total Pages | : 396 |
Release | : 1975 |
Genre | : Geothermal engineering |
ISBN | : |
The Geothermal Research Program of the U.S. Geological Survey
Author | : Wendell A. Duffield |
Publisher | : |
Total Pages | : 24 |
Release | : 1982 |
Genre | : Geothermal resources |
ISBN | : |
The Salton Sea Geothermal Field, California, as a Near-field Natural Analog of a Radioactive Waste Repository in Salt
Author | : W. A. Elders |
Publisher | : |
Total Pages | : 168 |
Release | : 1983 |
Genre | : Geochemistry |
ISBN | : |
Since high concentrations of radionuclides and high temperatures are not normally encountered in salt domes or beds, finding an exact geologic analog of expected near-field conditions in a mined nuclear waste repository in salt will be difficult. The Salton Sea Geothermal Field, however, provides an opportunity to investigate the migration and retardation of naturally occurring U, Th, Ra, Cs, Sr and other elements in hot brines which have been moving through clay-rich sedimentary rocks for up to 100,000 years. The more than thirty deep wells drilled in this field to produce steam for electrical generation penetrate sedimentary rocks containing concentrated brines where temperatures reach 365/sup 0/C at only 2 km depth. The brines are primarily Na, K, Ca chlorides with up to 25% of total dissolved solids; they also contain high concentrations of metals such as Fe, Mn, Li, Zn, and Pb. This report describes the geology, geophysics and geochemistry of this system as a prelude to a study of the mobility of naturally occurring radionuclides and radionuclide analogs within it. The aim of this study is to provide data to assist in validating quantitative models of repository behavior and to use in designing and evaluating waste packages and engineered barriers. 128 references, 33 figures, 13 tables.
Cooperative Geochemical Investigation of Geothermal Resources in the Imperial Valley and Yuma Areas. Final Report
Author | : |
Publisher | : |
Total Pages | : |
Release | : 1973 |
Genre | : |
ISBN | : |
Preliminary studies indicate that the Imperial Valley has a large geothermal potential. In order to delineate additional geothermal systems a chemical and isotopic investigation of samples from water wells, springs, and geothermal wells in the Imperial Valley and Yuma areas was conducted. Na, K, and Ca concentrations of nearly 200 well water, spring water, hot spring, and geothermal fluid samples from the Imperial Valley area were measured by atomic absorption spectrophotometry. Fournier and Truesdell's function was determined for each water sample. Suspected geothermal areas are identified. Hydrogen and oxygen isotope abundances were determined in order to determine and to identify the source of the water in the Mesa geothermal system. (JGB).